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The bay is situated on a geological fault between the Alma
Syncline and the Tarkhankut rise. Tectonic movements have formed various depositions within the bay and indicate a relative sea level increase of approximately 2 metres since the 1st millennium BCE. With regard to shipping it is relatively
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294:Евпатория. Масштаб: 1 : 100 000. Состояние местности на 1986 год. Издание 1988 год.
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Kutaisov, Vadim A.; Smekalova, Tat’jana N. (28 February 2022).
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245:"Coastal geoarchaeology of Kerkinitis"
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262:10.35595/2414-9179-2022-2-28-431-446
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196:Kezlev körfezi, Кезлев корьфези
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324:. You can help Knowledge by
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157:2 km (1.2 mi)
149:24 km (15 mi)
320:-related article is a
165:10 m (33 ft)
381:Bays of the Black Sea
223:shallow and exposed.
97:45.19250°N 33.37972°E
188:Євпаторійська бухта
180:Евпаторийская бухта
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198:) is a bay in the
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290:Лист карты
276:26 December
146:Max. length
100: /
75:Coordinates
376:Yevpatoria
365:Categories
227:References
204:Yevpatoria
154:Max. width
88:33°22′47″E
85:45°11′33″N
318:Black Sea
271:1760-8538
200:Black Sea
184:Ukrainian
68:Black Sea
292:L-36-103
64:Location
176:Russian
136:Ukraine
269:
208:Crimea
132:Russia
316:This
202:near
126:Basin
322:stub
278:2023
267:ISSN
253:2016
257:doi
367::
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